ATURCARA PROGRAM WACANA ARKEOLOGI MARITIM
14 APRIL 2016
AUDITORIUM,
INSTITUT OSEANOGRAFI DAN SEKITARAN,
UNIVERSITI MALAYSIA TERENGGANU
8.30 pagi –        Ketibaan dan pendaftaran
8.40 pagi –        Ketibaan Dif Kehormat dan Pengucaptama
8.50 pagi –        Ketibaan Naib Canselor, Universiti Malaysia Terengganu, YBhg. Prof. Dato’ Dr. Nor Aieni binti Haji Mokhtar
9.00 pagi –        Nyanyian lagu Negaraku dan UMT Cita Warisan.
– Bacaan Doa
– Ucapan Perasmian oleh Y.Bhg. Dato’ Naib Canselor, Universiti Malaysia Terengganu
9.35 pagi –        Lawatan ke Galeri Penyelidikan INOS
10.00 pagi –     Minum pagi
10.30 pagi –     Keynote 1 oleh Prof. Madya Dr. Asyaari bin Muhamad
11.15 pagi –       Keynote 2 oleh En. Kamarul Baharin bin A. Kasim
12.00 tghari –  Dialog Wacana Arkeologi Maritim
1.00 petang –   Makan Tengahari dan bersurai
billboard wacana arkeologi maritim email
 Video:
[youtube height=”315″ width=”560″]https://www.youtube.com/watch?v=VRSF1HP1UuU[/youtube]

Abstract

While the sinking formation of Antarctic Bottom Water (AABW) is well understood, how this bottom water "returns home" through upwelling within ocean basins, particularly the Indo-Pacific, remains shrouded in uncertainty. In the 1960s, Munk’s classic "Abyssal Recipes" theory sought to explain these abyssal flows, yet later observations exposed two significant conflicts with real-world data. In 2016, Ferrari, McDougall, and colleagues proposed the "Towards a New Abyssal Recipe" framework, introducing bottom boundary layer (BBL) upwelling to address Munk’s inconsistencies. Drawing on recent evidence of a potential cooling trend in the deep ocean, this talk revisits these debates, offering a fresh interpretation of Munk’s discrepancies and proposing a new mechanism for abyssal upwelling in the Indo-Pacific. It contributes to the ongoing quest to unravel how bottom waters complete their global journey.

Presented by: Prof. Dr. HAN Lei
Affiliation: China-ASEAN College of Marine Science, Xiamen University, Malaysia
Address: Sepang, Selangor, Malaysia

 

 

 

 

 

 

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